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Results:

• 11. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  improving management policies and practices by learning from the outcomes of implemented management strategies. Partici- patory integrated assessment is here a form of problem structuring for identification of gaps, ambiguity and multiple frames, confrontation, and integration of the most divergent views with respect to a given problem situation. Additional methods and tools that AM require com /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 12. Journal_of_Hydrology_Veijalainen_etal

  when the spring floods decreased and autumn and winter floods increased. The differences between the scenarios were estimated by com- paring the average changes of the scenarios (marked with dia- monds in Fig. 5). The differences between different emission scenarios with the same GCM were rather small; the average changes in floods differed on average by 1.7% units in 2070– 2099. The B1 scenario /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 13. VI_2020_005

  5 Conclusion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 60 References . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 61 Appendix: Description of the usage of the ACER method to find return periods and an adopted Hunter method to calculate allowances in Norway . . . . . . . . . . . . . . 73 1 Introduction The dynamic /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 14. Adalgeirsdottir-etal-tc-5-961-2011

  The Cryosphere, 5, 961–975, 2011 www.the-cryosphere.net/5/961/2011/ doi:10.5194/tc-5-961-2011 © Author(s) 2011. CC Attribution 3.0 License. The Cryosphere Modelling the 20th and 21st century evolution of Hoffellsjökull glacier, SE-Vatnajökull, Iceland G. Aðalgeirsdóttir1,2, S. Guðmundsson1, H. Björnsson1, F. Pálsson1, T. Jóhannesson3, H. Hannesdóttir1, S. Þ. Sigurðsson4, and E. Berthier5 /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 15. GA_2009_91A_4_Andreassen

  the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.pdf

• 16. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  Public Choice (2010) 143: 293–301 DOI 10.1007/s11127-010-9626-5 Foundations of the Ostrom workshop: institutional analysis, polycentricity, and self-governance of the commons Michael D. McGinnis · James M. Walker Received: 25 January 2010 / Accepted: 22 February 2010 / Published online: 8 April 2010 ³ Springer Science+Business Media, LLC 2010 Abstract This paper highlights important lessons /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 17. IPPC-2007-ar4_syr

  and their interactions with sustainable develop- Figure I.1. Schematic framework representing anthropogenic drivers, impacts of and responses to climate change, and their linkages. Schematic framework of anthropogenic climate change drivers, impacts and responses ment. Topic 5 assesses the relationship between adaptation and mitigation on a more conceptual basis and takes a longer-term per- spective. Topic 6 /media/loftslag/IPPC-2007-ar4_syr.pdf

• 18. VI_2009_006_tt

  to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 19. 2010_005_

  Temperature . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 17 4.2 Total Precipitation . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 19 5 Seasonal Differences in Climate Trends 20 6 Conclusions 21 5 List of Figures 1 Mean annual surface air temperature during the 1961–90 control period, differ- ences in degrees between the control period and the 2021–50 reference /media/ces/2010_005_.pdf

• 20. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  to determine a global figure for economic impact (From: EM-DAT 2008). 4 Based on baseline assessments of the case-studies in the NeWater- project (http://www.newater.info). 264 P. Huntjens et al. 123 these case-studies, more specifically in their level of AIWM.5 Therefore, this paper intends to identify differ- ences and similarities in AIWM, to detect general patterns, and to compare measures being /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf